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By Dr. Abdul Raof Jado, Prof. Dr. Josef Georg Zötl (auth.), Dr. Abdul Raof Jado, Prof. Dr. Josef Georg Zötl (eds.)
Read Online or Download Quaternary Period in Saudi Arabia: Volume 2 Sedimentological, Hydrogeological, Hydrochemical, Geomorphological, Geochronological, and Climatological Investigations in Western Saudi Arabia PDF
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Additional info for Quaternary Period in Saudi Arabia: Volume 2 Sedimentological, Hydrogeological, Hydrochemical, Geomorphological, Geochronological, and Climatological Investigations in Western Saudi Arabia
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54 centimeters. M. EYAL et al. (1981) and G. 5 centimeters per year. The lateral shear caused a further extension of the rearranged graben structure, with the opening of rhombic ally defined, en-echelon parts of the graben (Fig. 9). On the Gulf of Aqaba, the lateral strike slip itself includes a 60-kilometers shear in what today is the sea, and 50 kilometers in highly fault-structured shear belts on both sides of the Gulf. This extensive shearing along a number of paths of movement results in a whole system of block faults that in turn go through their own wedging or detaching movements.
This extensive shearing along a number of paths of movement results in a whole system of block faults that in turn go through their own wedging or detaching movements. The shearing in this entire region is characterized by tremendous horizontal paths of movement as well as large interlacing faults, in places with wide mylonite zones. 1. ::::1 o Precambrian basement CIJ Faults Cambrian-Quaternary [I] Basin by en-echelon faults Fig. 9. The shear along the Gulf of Aqaba with the development of the en-echelon basin structure (after R.
The steep sides of the wadis show that this second terrace is younger than the 10-meters terrace, as the layers of the former overlay those of the lower terrace. For this reason, these first and second morphological terraces may belong to the same cycle of change in relative sea level. There is an unconformity between these first two terraces and the third one. Beachrocks or gravels from the shore of the younger terrace are in onlap contact with the reef carbonates of the third terrace, which is now 16 meters above m.